NIVA Denmark Water Research, Ørestads Boulevard 73, 2300, Copenhagen S, Denmark.
Baltic Nest Institute, Aarhus University, Frederiksborgvej 399, 4000, Roskilde, Denmark.
Biol Rev Camb Philos Soc. 2017 Feb;92(1):135-149. doi: 10.1111/brv.12221. Epub 2015 Oct 14.
Much of the Baltic Sea is currently classified as 'affected by eutrophication'. The causes for this are twofold. First, current levels of nutrient inputs (nitrogen and phosphorus) from human activities exceed the natural processing capacity with an accumulation of nutrients in the Baltic Sea over the last 50-100 years. Secondly, the Baltic Sea is naturally susceptible to nutrient enrichment due to a combination of long retention times and stratification restricting ventilation of deep waters. Here, based on a unique data set collated from research activities and long-term monitoring programs, we report on the temporal and spatial trends of eutrophication status for the open Baltic Sea over a 112-year period using the HELCOM Eutrophication Assessment Tool (HEAT 3.0). Further, we analyse variation in the confidence of the eutrophication status assessment based on a systematic quantitative approach using coefficients of variation in the observations. The classifications in our assessment indicate that the first signs of eutrophication emerged in the mid-1950s and the central parts of the Baltic Sea changed from being unaffected by eutrophication to being affected. We document improvements in eutrophication status that are direct consequences of long-term efforts to reduce the inputs of nutrients. The reductions in both nitrogen and phosphorus loads have led to large-scale alleviation of eutrophication and to a healthier Baltic Sea. Reduced confidence in our assessment is seen more recently due to reductions in the scope of monitoring programs. Our study sets a baseline for implementation of the ecosystem-based management strategies and policies currently in place including the EU Marine Strategy Framework Directives and the HELCOM Baltic Sea Action Plan.
目前,波罗的海的大部分地区被归类为“受到富营养化影响”。造成这种情况的原因有两个。首先,人类活动中目前的营养物质(氮和磷)输入水平超过了自然处理能力,导致过去 50-100 年波罗的海中营养物质的积累。其次,由于滞留时间长和分层限制了深层水的通风,波罗的海本身容易受到营养物质富集的影响。在这里,我们根据从研究活动和长期监测计划中收集的独特数据集,使用 HELCOM 富营养化评估工具 (HEAT 3.0) 报告了过去 112 年波罗的海开阔海域富营养化状况的时空趋势。此外,我们还基于系统的定量方法,使用观测值的变异系数,分析了富营养化状况评估的置信度变化。我们的评估分类表明,富营养化的最初迹象出现在 20 世纪 50 年代中期,波罗的海中部地区从不受富营养化影响变为受到影响。我们记录了富营养化状况的改善,这是长期努力减少营养物质输入的直接结果。氮和磷负荷的减少导致了大规模的富营养化缓解和更健康的波罗的海。由于监测计划范围的缩小,我们的评估可信度最近有所降低。我们的研究为实施当前现有的基于生态系统的管理战略和政策奠定了基础,包括欧盟海洋战略框架指令和赫尔辛基委员会波罗的海行动计划。